|
| real(kind_phys), public | tau_g2r = 600. |
| | graupel melting to rain time scale (s)
|
| |
| real(kind_phys), public | tau_g2v = 900. |
| | graupel sublimation time scale (s)
|
| |
| real(kind_phys), public | tau_v2g = 21600. |
| | graupel deposition – make it a slow process time scale (s)
|
| |
| real(kind_phys), public | qc_crt = 5.0e-8 |
| | mini condensate mixing ratio to allow partial cloudiness
|
| |
| real(kind_phys), public | qr0_crt = 1.0e-4 |
| | rain to snow or graupel/hail threshold lfo used * mixing ratio * = 1.e-4 (hail in lfo)
|
| |
| real(kind_phys), public | c_piacr = 5.0 |
| | accretion: rain to ice:
|
| |
| real(kind_phys), public | c_cracw = 0.9 |
| | rain accretion efficiency
|
| |
| real(kind_phys), public | alin = 842.0 |
| | "a" in lin1983
|
| |
| real(kind_phys), public | clin = 4.8 |
| | "c" in lin 1983, 4.8 – > 6. (to ehance ql – > qs)
|
| |
| logical, public | fast_sat_adj = .false. |
| | has fast saturation adjustments
|
| |
| logical, public | use_ccn = .false. |
| | must be true when prog_ccn is false
|
| |
| logical, public | use_ppm = .false. |
| | use ppm fall scheme
|
| |
| logical, public | mono_prof = .true. |
| | perform terminal fall with mono ppm scheme
|
| |
| logical, public | mp_print = .false. |
| | cloud microphysics debugging printout
|
| |
| logical, public | de_ice = .false. |
| | to prevent excessive build - up of cloud ice from external sources
|
| |
| logical, public | sedi_transport = .true. |
| | transport of momentum in sedimentation
|
| |
| real(kind_phys), public | cld_min = 0.05 |
| | (v1/v3) minimum cloud fraction
|
| |
| real(kind_phys), public | t_min = 178. |
| | (v1/v3) min temp to freeze - dry all water vapor
|
| |
| real(kind_phys), public | t_sub = 184. |
| | (v1/v3) min temp for sublimation of cloud ice
|
| |
| real(kind_phys), public | mp_time = 150. |
| | (v1/v3) maximum micro - physics time step (sec)
|
| |
| real(kind_phys), public | rh_inc = 0.25 |
| | (v1/v3) rh increment for complete evaporation of cloud water and cloud ice
|
| |
| real(kind_phys), public | rh_inr = 0.25 |
| | (v1/v3) rh increment for minimum evaporation of rain
|
| |
| real(kind_phys), public | rh_ins = 0.25 |
| | (v1/v3) rh increment for sublimation of snow
|
| |
| real(kind_phys), public | tau_r2g = 900. |
| | (v1/v3) rain freezing during fast_sat time scale (s)
|
| |
| real(kind_phys), public | tau_smlt = 900. |
| | (v1/v3) snow melting time scale (s)
|
| |
| real(kind_phys), public | tau_i2s = 1000. |
| | (v1/v3) cloud ice to snow auto-conversion time scale (s)
|
| |
| real(kind_phys), public | tau_l2r = 900. |
| | (v1/v3) cloud water to rain auto-conversion time scale (s)
|
| |
| real(kind_phys), public | tau_v2l = 150. |
| | (v1/v3) water vapor to cloud water (condensation) time scale (s)
|
| |
| real(kind_phys), public | tau_l2v = 300. |
| | (v1/v3) cloud water to water vapor (evaporation) time scale (s)
|
| |
| real(kind_phys), public | dw_land = 0.20 |
| | (v1/v3) value for subgrid deviation / variability over land
|
| |
| real(kind_phys), public | dw_ocean = 0.10 |
| | (v1/v3) base value for ocean
|
| |
| real(kind_phys), public | ccn_o = 90. |
| | (v1/v3) ccn over ocean (cm^ - 3)
|
| |
| real(kind_phys), public | ccn_l = 270. |
| | (v1/v3) ccn over land (cm^ - 3)
|
| |
| real(kind_phys), public | sat_adj0 = 0.90 |
| | (v1/v3) adjustment factor (0: no, 1: full) during fast_sat_adj
|
| |
| real(kind_phys), public | qi_lim = 1. |
| | (v1/v3) cloud ice limiter (0: no, 1: full, >1: extra) to prevent large ice build up
|
| |
| real(kind_phys), public | ql_mlt = 2.0e-3 |
| | (v1/v3) max value of cloud water allowed from melted cloud ice
|
| |
| real(kind_phys), public | qs_mlt = 1.0e-6 |
| | (v1/v3) max cloud water due to snow melt
|
| |
| real(kind_phys), public | ql_gen = 1.0e-3 |
| | (v1/v3) max cloud water generation during remapping step if fast_sat_adj = .t.
|
| |
| real(kind_phys), public | qi_gen = 1.82e-6 |
| | (v1/v3) max cloud ice generation during remapping step (V1 ONLY. Computed internally in V3)
|
| |
| real(kind_phys), public | ql0_max = 2.0e-3 |
| | (v1/v3) max cloud water value (auto converted to rain)
|
| |
| real(kind_phys), public | qi0_max = 1.0e-4 |
| | (v1/v3) max cloud ice value (by other sources)
|
| |
| real(kind_phys), public | qi0_crt = 1.0e-4 |
| | (v1/v3) cloud ice to snow autoconversion threshold (was 1.e-4); qi0_crt is highly dependent on horizontal resolution
|
| |
| real(kind_phys), public | qs0_crt = 1.0e-3 |
| | (v1/v3) snow to graupel density threshold (0.6e-3 in purdue lin scheme)
|
| |
| real(kind_phys), public | c_paut = 0.55 |
| | (v1/v3) autoconversion cloud water to rain (use 0.5 to reduce autoconversion)
|
| |
| real(kind_phys), public | vi_fac = 1. |
| | (v1/v3) if const_vi: 1 / 3
|
| |
| real(kind_phys), public | vs_fac = 1. |
| | (v1/v3) if const_vs: 1.
|
| |
| real(kind_phys), public | vg_fac = 1. |
| | (v1/v3) if const_vg: 2.
|
| |
| real(kind_phys), public | vr_fac = 1. |
| | (v1/v3) if const_vr: 4.
|
| |
| real(kind_phys), public | vr_max = 12. |
| | (v1/v3) max fall speed for rain
|
| |
| real(kind_phys), public | rewmin = 5.0 |
| | (v1/v3) minimum effective radii (liquid)
|
| |
| real(kind_phys), public | reimin = 10.0 |
| | (v1/v3) minimum effective radii (ice)
|
| |
| real(kind_phys), public | reimax = 150.0 |
| | (v1/v3) maximum effective radii (ice)
|
| |
| real(kind_phys), public | rermax = 10000.0 |
| | (v1/v3) maximum effective radii (rain)
|
| |
| real(kind_phys), public | resmin = 150.0 |
| | (v1/v3) minimum effective radii (snow)
|
| |
| real(kind_phys), public | resmax = 10000.0 |
| | (v1/v3) maximum effective radii (snow)
|
| |
| real(kind_phys), public | regmax = 10000.0 |
| | (v1/v3) maximum effective radii (graupel)
|
| |
| logical, public | const_vi = .false. |
| | (v1/v3) if .t. the constants are specified by v * _fac
|
| |
| logical, public | const_vs = .false. |
| | (v1/v3) if .t. the constants are specified by v * _fac
|
| |
| logical, public | const_vg = .false. |
| | (v1/v3) if .t. the constants are specified by v * _fac
|
| |
| logical, public | const_vr = .false. |
| | (v1/v3) if .t. the constants are specified by v * _fac
|
| |
| logical, public | z_slope_liq = .true. |
| | (v1/v3) use linear mono slope for autocconversions
|
| |
| logical, public | do_hail = .false. |
| | (v1/v3) use hail parameters instead of graupel
|
| |
| logical, public | do_qa = .true. |
| | (v1/v3) do inline cloud fraction
|
| |
| logical, public | rad_snow = .true. |
| | (v1/v3) consider snow in cloud fraciton calculation
|
| |
| logical, public | rad_graupel = .true. |
| | (v1/v3) consider graupel in cloud fraction calculation
|
| |
| logical, public | rad_rain = .true. |
| | (v1/v3) consider rain in cloud fraction calculation
|
| |
| logical, public | do_sedi_heat = .true. |
| | (v1/v3) transport of heat in sedimentation
|
| |
| logical, public | prog_ccn = .false. |
| | (v1/v3) do prognostic ccn (yi ming's method)
|
| |
| logical, public | tintqs = .false. |
| | (v1/v3)
|
| |
| integer, public | icloud_f = 0 |
| | (v1/v3) GFDL cloud scheme 0: subgrid variability based scheme 1: same as 0, but for old fvgfs implementation 2: binary cloud scheme 3: extension of 0
|
| |
| integer, public | irain_f = 0 |
| | (v1/v3) cloud water to rain auto conversion scheme 0: subgrid variability based scheme 1: no subgrid varaibility
|
| |
| real(kind_phys), public | tice = 273.16 |
| | freezing temperature (K): ref: GFDL, GFS (DJS: V3=273.15)
|
| |
| real(kind_phys), public | tau_imlt = 600. |
| | cloud ice melting time scale (s) (DJS: V3=1200.)
|
| |
| real(kind_phys), public | rthresh = 10.0e-6 |
| | critical cloud drop radius (micro m) (DJS: v3=20.0e-6)
|
| |
| real(kind_phys), public | c_psaci = 0.02 |
| | accretion: cloud ice to snow (was 0.1 in zetac) (DJS: v3=0.05)
|
| |
| real(kind_phys), public | c_pgacs = 2.0e-3 |
| | snow to graupel "accretion" eff. (was 0.1 in zetac) (DJS: v3=0.01)
|
| |
| real(kind_phys), public | vi_max = 0.5 |
| | max fall speed for ice (DJS: v3=1.0)
|
| |
| real(kind_phys), public | vs_max = 5.0 |
| | max fall speed for snow (DJS: v3=2.0)
|
| |
| real(kind_phys), public | vg_max = 8.0 |
| | max fall speed for graupel (DJS: v3=12.0)
|
| |
| real(kind_phys), public | rewmax = 10.0 |
| | maximum effective radii (liquid) (DJS: v3=15.0)
|
| |
| real(kind_phys), public | rermin = 10.0 |
| | minimum effective radii (rain) (DJS: v3=15.0)
|
| |
| real(kind_phys), public | regmin = 300.0 |
| | minimum effective radii (graupel) (DJS: v3=150.0)
|
| |
| logical, public | z_slope_ice = .false. |
| | use linear mono slope for autocconversions (DJS: v3=.true.)
|
| |
| logical, public | do_sedi_w = .false. |
| | transport of vertical motion in sedimentation (DJS: v3=.true.)
|
| |
| logical, public | fix_negative = .false. |
| | fix negative water species (DJS: v3=.true.)
|
| |
| integer, public | reiflag = 1 |
| | cloud ice effective radius scheme (DJS: v3=5) 1: Heymsfield and Mcfarquhar (1996) 2: Donner et al. (1997) 3: Fu (2007) 4: Kristjansson et al. (2000) 5: Wyser (1998) 6: Sun and Rikus (1999), Sun (2001) 7: effective radius
|
| |
| logical, public | const_vw = .false. |
| | if .ture., the constants are specified by v * _fac
|
| |
| logical, public | do_sedi_uv = .true. |
| | transport of horizontal momentum in sedimentation
|
| |
| logical, public | do_sedi_melt = .true. |
| | melt cloud ice, snow, and graupel during sedimentation
|
| |
| logical, public | liq_ice_combine = .false. |
| | combine all liquid water, combine all solid water
|
| |
| logical, public | snow_grauple_combine = .true. |
| | combine snow and graupel
|
| |
| logical, public | use_rhc_cevap = .false. |
| | cap of rh for cloud water evaporation
|
| |
| logical, public | use_rhc_revap = .false. |
| | cap of rh for rain evaporation
|
| |
| logical, public | do_cld_adj = .false. |
| | do cloud fraction adjustment
|
| |
| logical, public | do_evap_timescale = .true. |
| | whether to apply a timescale to evaporation
|
| |
| logical, public | do_cond_timescale = .false. |
| | whether to apply a timescale to condensation
|
| |
| logical, public | consv_checker = .false. |
| | turn on energy and water conservation checker
|
| |
| logical, public | do_warm_rain_mp = .false. |
| | do warm rain cloud microphysics only
|
| |
| logical, public | do_wbf = .false. |
| | do Wegener Bergeron Findeisen process
|
| |
| logical, public | do_psd_water_fall = .false. |
| | calculate cloud water terminal velocity based on PSD
|
| |
| logical, public | do_psd_ice_fall = .false. |
| | calculate cloud ice terminal velocity based on PSD
|
| |
| logical, public | do_psd_water_num = .false. |
| | calculate cloud water number concentration based on PSD
|
| |
| logical, public | do_psd_ice_num = .false. |
| | calculate cloud ice number concentration based on PSD
|
| |
| logical, public | do_new_acc_water = .false. |
| | perform the new accretion for cloud water
|
| |
| logical, public | do_new_acc_ice = .false. |
| | perform the new accretion for cloud ice
|
| |
| logical, public | cp_heating = .false. |
| | update temperature based on constant pressure
|
| |
| logical, public | delay_cond_evap = .false. |
| | do condensation evaporation only at the last time step
|
| |
| logical, public | do_subgrid_proc = .true. |
| | do temperature sentive high vertical resolution processes
|
| |
| logical, public | fast_fr_mlt = .true. |
| | do freezing and melting in fast microphysics
|
| |
| logical, public | fast_dep_sub = .true. |
| | do deposition and sublimation in fast microphysics
|
| |
| integer, public | ntimes = 1 |
| | cloud microphysics sub cycles
|
| |
| integer, public | nconds = 1 |
| | condensation sub cycles
|
| |
| integer, public | inflag = 1 |
| | ice nucleation scheme 1: Hong et al. (2004) 2: Meyers et al. (1992) 3: Meyers et al. (1992) 4: Cooper (1986) 5: Fletcher (1962)
|
| |
| integer, public | igflag = 3 |
| | ice generation scheme 1: WSM6 2: WSM6 with 0 at 0 C 3: WSM6 with 0 at 0 C and fixed value at - 10 C 4: combination of 1 and 3
|
| |
| integer, public | ifflag = 1 |
| | ice fall scheme 1: Deng and Mace (2008) 2: Heymsfield and Donner (1990)
|
| |
| integer, public | rewflag = 1 |
| | cloud water effective radius scheme 1: Martin et al. (1994) 2: Martin et al. (1994), GFDL revision 3: Kiehl et al. (1994) 4: effective radius
|
| |
| integer, public | rerflag = 1 |
| | rain effective radius scheme 1: effective radius
|
| |
| integer, public | resflag = 1 |
| | snow effective radius scheme 1: effective radius
|
| |
| integer, public | regflag = 1 |
| | graupel effective radius scheme 1: effective radius
|
| |
| integer, public | radr_flag = 1 |
| | radar reflectivity for rain 1: Mark Stoelinga (2005) 2: Smith et al. (1975), Tong and Xue (2005) 3: Marshall-Palmer formula (https://en.wikipedia.org/wiki/DBZ_(meteorology))
|
| |
| integer, public | rads_flag = 1 |
| | radar reflectivity for snow 1: Mark Stoelinga (2005) 2: Smith et al. (1975), Tong and Xue (2005) 3: Marshall-Palmer formula (https://en.wikipedia.org/wiki/DBZ_(meteorology))
|
| |
| integer, public | radg_flag = 1 |
| | radar reflectivity for graupel 1: Mark Stoelinga (2005) 2: Smith et al. (1975), Tong and Xue (2005) 3: Marshall-Palmer formula (https://en.wikipedia.org/wiki/DBZ_(meteorology))
|
| |
| integer, public | sedflag = 1 |
| | sedimentation scheme 1: implicit scheme 2: explicit scheme 3: lagrangian scheme 4: combined implicit and lagrangian scheme
|
| |
| integer, public | vdiffflag = 1 |
| | wind difference scheme in accretion 1: Wisner et al. (1972) 2: Mizuno (1990) 3: Murakami (1990)
|
| |
| real(kind_phys), public | c_psacw = 1.0 |
| | cloud water to snow accretion efficiency
|
| |
| real(kind_phys), public | c_pracw = 0.8 |
| | cloud water to rain accretion efficiency
|
| |
| real(kind_phys), public | c_praci = 1.0 |
| | cloud ice to rain accretion efficiency
|
| |
| real(kind_phys), public | c_pgacw = 1.0 |
| | cloud water to graupel accretion efficiency
|
| |
| real(kind_phys), public | c_pgaci = 0.05 |
| | cloud ice to graupel accretion efficiency (was 0.1 in ZETAC)
|
| |
| real(kind_phys), public | c_pracs = 1.0 |
| | snow to rain accretion efficiency
|
| |
| real(kind_phys), public | c_psacr = 1.0 |
| | rain to snow accretion efficiency
|
| |
| real(kind_phys), public | c_pgacr = 1.0 |
| | rain to graupel accretion efficiency
|
| |
| real(kind_phys), public | alinw = 3.e7 |
| | "a" in Lin et al. (1983) for cloud water (Ikawa and Saito 1990)
|
| |
| real(kind_phys), public | alini = 7.e2 |
| | "a" in Lin et al. (1983) for cloud ice (Ikawa and Saita 1990)
|
| |
| real(kind_phys), public | alinr = 842.0 |
| | "a" in Lin et al. (1983) for rain (Liu and Orville 1969)
|
| |
| real(kind_phys), public | alins = 4.8 |
| | "a" in Lin et al. (1983) for snow (straka 2009)
|
| |
| real(kind_phys), public | aling = 1.0 |
| | "a" in Lin et al. (1983), similar to a, but for graupel (Pruppacher and Klett 2010)
|
| |
| real(kind_phys), public | alinh = 1.0 |
| | "a" in Lin et al. (1983), similar to a, but for hail (Pruppacher and Klett 2010)
|
| |
| real(kind_phys), public | blinw = 2.0 |
| | "b" in Lin et al. (1983) for cloud water (Ikawa and Saito 1990)
|
| |
| real(kind_phys), public | blini = 1.0 |
| | "b" in Lin et al. (1983) for cloud ice (Ikawa and Saita 1990)
|
| |
| real(kind_phys), public | blinr = 0.8 |
| | "b" in Lin et al. (1983) for rain (Liu and Orville 1969)
|
| |
| real(kind_phys), public | blins = 0.25 |
| | "b" in Lin et al. (1983) for snow (straka 2009)
|
| |
| real(kind_phys), public | bling = 0.5 |
| | "b" in Lin et al. (1983), similar to b, but for graupel (Pruppacher and Klett 2010)
|
| |
| real(kind_phys), public | blinh = 0.5 |
| | "b" in Lin et al. (1983), similar to b, but for hail (Pruppacher and Klett 2010)
|
| |
| real(kind_phys), public | vw_fac = 1.0 |
| |
| real(kind_phys), public | vw_max = 0.01 |
| | maximum fall speed for cloud water (m/s)
|
| |
| real(kind_phys), public | tice_mlt = 273.16 |
| | can set ice melting temperature to 268 based on observation (Kay et al. 2016) (K)
|
| |
| real(kind_phys), public | tau_gmlt = 600.0 |
| | graupel melting time scale (s)
|
| |
| real(kind_phys), public | tau_wbf = 300.0 |
| | graupel melting time scale (s)
|
| |
| real(kind_phys), public | tau_revp = 0.0 |
| | rain evaporation time scale (s)
|
| |
| real(kind_phys), public | is_fac = 0.2 |
| | cloud ice sublimation temperature factor
|
| |
| real(kind_phys), public | ss_fac = 0.2 |
| | snow sublimation temperature factor
|
| |
| real(kind_phys), public | gs_fac = 0.2 |
| | graupel sublimation temperature factor
|
| |
| real(kind_phys), public | rh_fac_evap = 10.0 |
| | cloud water evaporation relative humidity factor
|
| |
| real(kind_phys), public | rh_fac_cond = 10.0 |
| | cloud water condensation relative humidity factor
|
| |
| real(kind_phys), public | sed_fac = 1.0 |
| | coefficient for sedimentation fall, scale from 1.0 (implicit) to 0.0 (lagrangian)
|
| |
| real(kind_phys), public | xr_a = 0.25 |
| | p value in Xu and Randall (1996)
|
| |
| real(kind_phys), public | xr_b = 100.0 |
| | alpha_0 value in Xu and Randall (1996)
|
| |
| real(kind_phys), public | xr_c = 0.49 |
| | gamma value in Xu and Randall (1996)
|
| |
| real(kind_phys), public | te_err = 1.e-5 |
| | 64bit: 1.e-14, 32bit: 1.e-7; turn off to save computer time
|
| |
| real(kind_phys), public | tw_err = 1.e-8 |
| | 64bit: 1.e-14, 32bit: 1.e-7; turn off to save computer time
|
| |
| real(kind_phys), public | rh_thres = 0.75 |
| | minimum relative humidity for cloud fraction
|
| |
| real(kind_phys), public | rhc_cevap = 0.85 |
| | maximum relative humidity for cloud water evaporation
|
| |
| real(kind_phys), public | rhc_revap = 0.85 |
| | maximum relative humidity for rain evaporation
|
| |
| real(kind_phys), public | f_dq_p = 1.0 |
| | cloud fraction adjustment for supersaturation
|
| |
| real(kind_phys), public | f_dq_m = 1.0 |
| | cloud fraction adjustment for undersaturation
|
| |
| real(kind_phys), public | fi2s_fac = 1.0 |
| | maximum sink of cloud ice to form snow: 0-1
|
| |
| real(kind_phys), public | fi2g_fac = 1.0 |
| | maximum sink of cloud ice to form graupel: 0-1
|
| |
| real(kind_phys), public | fs2g_fac = 1.0 |
| | maximum sink of snow to form graupel: 0-1
|
| |
| real(kind_phys), public | n0w_sig = 1.1 |
| | intercept parameter (significand) of cloud water (Lin et al. 1983) (1/m^4) (Martin et al. 1994)
|
| |
| real(kind_phys), public | n0i_sig = 1.3 |
| | intercept parameter (significand) of cloud ice (Lin et al. 1983) (1/m^4) (McFarquhar et al. 2015)
|
| |
| real(kind_phys), public | n0r_sig = 8.0 |
| | intercept parameter (significand) of rain (Lin et al. 1983) (1/m^4) (Marshall and Palmer 1948)
|
| |
| real(kind_phys), public | n0s_sig = 3.0 |
| | intercept parameter (significand) of snow (Lin et al. 1983) (1/m^4) (Gunn and Marshall 1958)
|
| |
| real(kind_phys), public | n0g_sig = 4.0 |
| | intercept parameter (significand) of graupel (Rutledge and Hobbs 1984) (1/m^4) (Houze et al. 1979)
|
| |
| real(kind_phys), public | n0h_sig = 4.0 |
| | intercept parameter (significand) of hail (Lin et al. 1983) (1/m^4) (Federer and Waldvogel 1975)
|
| |
| real(kind_phys), public | n0w_exp = 41 |
| | intercept parameter (exponent) of cloud water (Lin et al. 1983) (1/m^4) (Martin et al. 1994)
|
| |
| real(kind_phys), public | n0i_exp = 18 |
| | intercept parameter (exponent) of cloud ice (Lin et al. 1983) (1/m^4) (McFarquhar et al. 2015)
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| real(kind_phys), public | n0r_exp = 6 |
| | intercept parameter (exponent) of rain (Lin et al. 1983) (1/m^4) (Marshall and Palmer 1948)
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| real(kind_phys), public | n0s_exp = 6 |
| | intercept parameter (exponent) of snow (Lin et al. 1983) (1/m^4) (Gunn and Marshall 1958)
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| real(kind_phys), public | n0g_exp = 6 |
| | intercept parameter (exponent) of graupel (Rutledge and Hobbs 1984) (1/m^4) (Houze et al. 1979)
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| real(kind_phys), public | n0h_exp = 4 |
| | intercept parameter (exponent) of hail (Lin et al. 1983) (1/m^4) (Federer and Waldvogel 1975)
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| real(kind_phys), public | muw = 6.0 |
| | shape parameter of cloud water in Gamma distribution (Martin et al. 1994)
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| real(kind_phys), public | mui = 3.35 |
| | shape parameter of cloud ice in Gamma distribution (McFarquhar et al. 2015)
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| real(kind_phys), public | mur = 1.0 |
| | shape parameter of rain in Gamma distribution (Marshall and Palmer 1948)
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| real(kind_phys), public | mus = 1.0 |
| | shape parameter of snow in Gamma distribution (Gunn and Marshall 1958)
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| real(kind_phys), public | mug = 1.0 |
| | shape parameter of graupel in Gamma distribution (Houze et al. 1979)
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| real(kind_phys), public | muh = 1.0 |
| | shape parameter of hail in Gamma distribution (Federer and Waldvogel 1975)
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| real(kind_phys), public | beta = 1.22 |
| | defined in Heymsfield and Mcfarquhar (1996)
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| real(kind_phys), public | rewfac = 1.0 |
| | this is a tuning parameter to compromise the inconsistency between GFDL MP's PSD and cloud water radiative property's PSD assumption. after the cloud water radiative property's PSD is rebuilt, this parameter should be 1.0.
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| real(kind_phys), public | reifac = 1.0 |
| | this is a tuning parameter to compromise the inconsistency between GFDL MP's PSD and cloud ice radiative property's PSD assumption. after the cloud ice radiative property's PSD is rebuilt, this parameter should be 1.0.
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